全文获取类型
收费全文 | 16357篇 |
免费 | 2194篇 |
国内免费 | 2767篇 |
专业分类
测绘学 | 5033篇 |
大气科学 | 3770篇 |
地球物理 | 2513篇 |
地质学 | 3081篇 |
海洋学 | 2051篇 |
天文学 | 1474篇 |
综合类 | 1499篇 |
自然地理 | 1897篇 |
出版年
2024年 | 84篇 |
2023年 | 215篇 |
2022年 | 548篇 |
2021年 | 706篇 |
2020年 | 718篇 |
2019年 | 867篇 |
2018年 | 598篇 |
2017年 | 900篇 |
2016年 | 799篇 |
2015年 | 825篇 |
2014年 | 979篇 |
2013年 | 1185篇 |
2012年 | 1091篇 |
2011年 | 1025篇 |
2010年 | 780篇 |
2009年 | 1002篇 |
2008年 | 984篇 |
2007年 | 1187篇 |
2006年 | 1073篇 |
2005年 | 871篇 |
2004年 | 809篇 |
2003年 | 645篇 |
2002年 | 553篇 |
2001年 | 451篇 |
2000年 | 399篇 |
1999年 | 337篇 |
1998年 | 279篇 |
1997年 | 204篇 |
1996年 | 217篇 |
1995年 | 191篇 |
1994年 | 163篇 |
1993年 | 158篇 |
1992年 | 99篇 |
1991年 | 87篇 |
1990年 | 50篇 |
1989年 | 50篇 |
1988年 | 35篇 |
1987年 | 27篇 |
1986年 | 19篇 |
1985年 | 16篇 |
1984年 | 16篇 |
1983年 | 5篇 |
1982年 | 10篇 |
1981年 | 8篇 |
1980年 | 7篇 |
1979年 | 5篇 |
1977年 | 12篇 |
1972年 | 4篇 |
1971年 | 5篇 |
1954年 | 7篇 |
排序方式: 共有10000条查询结果,搜索用时 765 毫秒
81.
Temperature data from 18 measurement series obtained during logging of the Oseberg field in the northern North Sea are presented. Because the measurement series are taken at approximately the same depth, they should give identical temperatures after depth correction, and are suitable for assessing the performance of different models used to determine virgin rock temperatures from well log information.We have used this data set to test the properties of the different models given by Shen and Beck (1986). Although these models were built to simulate closely the thermal recovery of a well and are unbiased, the uncertainties in the temperature estimates when applied to real data are found to be no less than those from simpler (biased) models. This fact confirms the conclusion of Hermanrud (1989a) who showed that physical factors other than those presently accounted for significantly influence the thermal recovery of a borehole. 相似文献
82.
83.
Weather in the North Gulf of Alaska is characterized by a high frequency of deep synoptic-scale low-pressure systems, especially during the cold season. The strong pressure gradients of these storms interact with the extremely rugged terrain of the coastal mountains to produce a variety of channeled flows. These surface wind regimes are not well documented in the scientific community, due to the paucity of observations. Modeling of these phenomena in regions of complex terrain is of great interest to those working with hydrodynamic, wave, and pollutant transport models in coastal and shelf areas. Such models, when coupled with ocean and coastal-ecology counterparts, give a broad view of the role surface winds play in shaping local coastal marine ecosystem in this region. This paper presents a climatology of simulated low-level wind jets over the domain of Cook Inlet and Shelikof Strait along Alaska's south-central coast. Daily simulations using the RAMS model were conducted in a 36-h forecast mode for the cold-season period 10/1/03 to 3/31/04. Systematic analysis of the resulting simulated low-level wind field makes it possible to characterize these jets and gap flows in spatial and temporal detail. The comparison between the RAMS winds and the Synthetic Aperture Radar (SAR)-derived winds when available verifies the existence of these wind jets and the capability of the model to simulate these cases. Clearly, the results of a study in this region depend on the fidelity of the model at these scales (O[5 km]). The SAR comparisons attempt to help establish this. From the 6 months of simulations over Cook Inlet and Shelikof Strait, the low-level wind jets are classified into 10 different regimes by location and orientation. These regimes are categorized into four more general groups: cross-channel westerly, easterly, and up and down Inlet flows. The nature of a particular regime is largely a function of pressure gradient orientation and local topography. Jets in the same group have a similar occurrence distribution with time. Some form of jet occurred in the study region almost daily each month of the period, with December 2003 having the highest frequency of wind jets. 相似文献
84.
85.
用北太平洋(含赤道太平洋区)1949~1979年的COADS资料,通过矢量EOF分解得到北太平洋异常风场的分布型及其时间变化规律。分析表明,EOF1~5场与大气活动中心、海洋相互作用有联系,具有明显的天气学意义。此外,还讨论了EOF异常风场间的转换及其季节性差异。 相似文献
86.
87.
通过分析1980年以后的海冰资料和卫星云图照片,对黄、渤海沿岸11个海冰测点的历史变迁进行了评述,浅析了测点的优劣及使用资料时应注意的事项。 相似文献
88.
We have examined wind-induced circulation in the Sea of Okhotsk using a barotropic model that contains realistic topography
with a resolution of 9.25 km. The monthly wind stress field calculated from daily European Centre for Medium-Range Weather
Forecasting (ECMWF) Re-Analysis data is used as the forcing, and the integration is carried out for 20 days until the circulation
attains an almost steady state. In the case of November (a representative for the winter season from October to March), southward
currents of velocity 0.1–0.3 m s−1 occur along the bottom contours off the east of Sakhalin Island. The currents are mostly confined to the shelf (shallower
than 200 m) and extend as far south as the Hokkaido coast. In the July case (a representative for the summer season from April
to September), significant currents do not occur, even in the shallow shelves. The simulated southward current over the east
Sakhalin shelf appears to correspond to the near-shore branch of the East Sakhalin Current (ESC), which was observed with
the surface drifters. These seasonal variations simulated in our experiments are consistent with the observations of the ESC.
Dynamically, the simulated ESC is interpreted as the arrested topographic wave (ATW), which is the coastally trapped flow
driven by steady alongshore wind stress. The volume transport of the simulated ESC over the shelf reaches about 1.0 Sv (1
Sv = 106 m3s−1) in the winter season, which is determined by the integrated onshore Ekman transport in the direction from which shelf waves
propagate.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
89.
90.
区域海洋地质数据库建设纲要 总被引:5,自引:0,他引:5
区域海洋地质数据库是中国地质调查局基础数据库的一个重要组成部分,是实现地质调查基础性与公益性战略部署的依托。根据区域海洋地质数据库建设的目标与任务,在数据结构和实施步骤等方面进行了初步研究。区域海洋地质数据库及其管理信息系统适合采取基于Web系统的三层体系结构,在数据构成上亦分为区域海洋地质调查原始资料与成果资料,其中元数据库的建设对数据库的应用非常重要,用户可以通过元数据了解数据的存在性、适宜性、有效性等,确定数据的使用方法,因此,元数据库的建设应采用国际已经普遍认可的ISO/TC211发布的ISO19115空间元数据标准。 相似文献